"[This book] should be of interest to a wide range of scientists concerned with the Earth, environmental and ecological sciences, including those specialising in the Holocene.

Stuart Harris and his co-authors provide a[...] comprehensive survey of the closely related field of geocryology. This is defined as the study of frozen ground, especially permafrost. Their book also includes the characteristics, processes, landforms and environmental factors affecting frozen ground, to which they add a wide variety of practical problems encountered by engineers and others who attempt to occupy and use permafrost terrain.

Part III of Geocryology is a superb demonstration, in the context of geocryology, of the intimate, reciprocal relationship that can exist between pure and applied science. Much of the detailed information and theoretical knowledge that underpins present understanding of frozen ground was developed hand in hand with relatively recent attempts to live in and exploit the resources available in permafrost areas."

John A Matthews, Swansea University,UK. In: The Holocene Vol. 28(4) (2018).

"With three co-authors who come from different countries to share their research experience and expertise, this book makes available geocryological information not published originally in the English language. As expected, the book is well endowed with case studies and illustrative examples taken mostly from northern Canada, Alaska, Siberia, and Tibet in China. These are a major attraction of this publication.

[...]

Overall, it is comprehensive and places geomorphology and geotechnical engineering under a single cover. As cold regions in general, and circumpolar areas in particular, are highly sensitive to changes due to natural and human-related causes, this book offers materials valuable to understanding and confronting present and future environmental changes. Without rendering quantitative treatment on many topics (except Chapter 12 on soil mechanics), the descriptive approach makes the book easily accessible to a general readership, and it will appeal to undergraduate students who are not mathematically inclined. Those who wish to pursue specific topics at greater depth can consult relevant articles listed in the very extensive bibliography, which covers 119 pages."

Ming-ko Woo, Professor Emeritus at the School of Geography and Earth Sciences, McMaster University, Canada. Published in: Arctic, Vol. 71(2) (2018).

"Overall, therefore, I found the book to be partially successful in its purpose. It does provide a welcome survey of modern geocryology, at least on a descriptive basis, but lacks rigor in terms of providing mechanistic understanding of processes and modeling. I recommend the book to university students, academics, consultant engineers and land managers because it makes a substantial contribution to the study of permafrost. By focusing on geocryological description, it complements the lucid summary of geocryological processes by Peter Williams and Michael Smith."

Julian B. Murton, Permafrost and Periglacial Processes 2018 (29): 131-132 "[This book] should be of interest to a wide range of scientists concerned with the Earth, environmental and ecological sciences, including those specialising in the Holocene.

Stuart Harris and his co-authors provide a[...] comprehensive survey of the closely related field of geocryology. This is defined as the study of frozen ground, especially permafrost. Their book also includes the characteristics, processes, landforms and environmental factors affecting frozen ground, to which they add a wide variety of practical problems encountered by engineers and others who attempt to occupy and use permafrost terrain.

Part III of Geocryology is a superb demonstration, in the context of geocryology, of the intimate, reciprocal relationship that can exist between pure and applied science. Much of the detailed information and theoretical knowledge that underpins present understanding of frozen ground was developed hand in hand with relatively recent attempts to live in and exploit the resources available in permafrost areas."

John A Matthews, Swansea University,UK. In: The Holocene Vol. 28(4) (2018).

"With three co-authors who come from different countries to share their research experience and expertise, this book makes available geocryological information not published originally in the English language. As expected, the book is well endowed with case studies and illustrative examples taken mostly from northern Canada, Alaska, Siberia, and Tibet in China. These are a major attraction of this publication.

[...]

Overall, it is comprehensive and places geomorphology and geotechnical engineering under a single cover. As cold regions in general, and circumpolar areas in particular, are highly sensitive to changes due to natural and human-related causes, this book offers materials valuable to understanding and confronting present and future environmental changes. Without rendering quantitative treatment on many topics (except Chapter 12 on soil mechanics), the descriptive approach makes the book easily accessible to a general readership, and it will appeal to undergraduate students who are not mathematically inclined. Those who wish to pursue specific topics at greater depth can consult relevant articles listed in the very extensive bibliography, which covers 119 pages."

Ming-ko Woo, Professor Emeritus at the School of Geography and Earth Sciences, McMaster University, Canada. Published in: Arctic, Vol. 71(2) (2018).

"Overall, therefore, I found the book to be partially successful in its purpose. It does provide a welcome survey of modern geocryology, at least on a descriptive basis, but lacks rigor in terms of providing mechanistic understanding of processes and modeling. I recommend the book to university students, academics, consultant engineers and land managers because it makes a substantial contribution to the study of permafrost. By focusing on geocryological description, it complements the lucid summary of geocryological processes by Peter Williams and Michael Smith."

Julian B. Murton, Permafrost and Periglacial Processes 2018 (29): 131-132